Connellite specimens for sale

4 for sale · $250–$9,500 USD

7 in the gallery

Connellite is a copper sulfate chloride mineral that forms as blue-green crystals and sometimes crusts or botryoidal masses. It typically displays a vitreous to submetallic luster and can occur in radiating or tabular crystal habits, revealing its distinctive aural-like edges in hand specimens. The mineral’s composition includes copper, sulfate, chloride, and water, contributing to its characteristic color and hydration state, while localities have produced well-formed crystals and attractive aggregates. Classic specimens come from notable localities in the United Kingdom and the United States, with other important sources in Russia that have yielded vivid, well-terminated crystals.

Formula
Cu19(SO4)(OH)32Cl4 · 3H2O
Rarity
Rare
Stability
Moderately Stable
Collector interest
High Interest
Classification notes
Sulfates (copper) with hydroxide and chloride; IMA group not specified

Key characteristics

Crystal system
hexagonal
Mohs hardness
3
Specific gravity
3.36–3.41
Luster
vitreous, silky
Transparency
transparent, translucent
Color
blue, green
Streak
blue
Cleavage
none
Fracture
uneven
Crystal habit
prismatic, acicular, fibrous, radiating, massive
  • Classic / historic

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Where Connellite is found

Top localities

  1. Wheal Gorland2 specimens
  2. Bagdad Mine1 specimen
  3. Bisbee1 specimen
  4. Rubtsovsk Mine1 specimen
  5. Southwest Mine1 specimen
  6. Wheal Cock1 specimen

About Connellite

Collectors prize connellite for its crisp crystal forms and the rarity of well-preserved sulfate chloride minerals in copper-rich environments. Fine pieces show sharp terminations and delicate blue-green color, often contrasting with darker matrix material. Its association with secondary copper deposits and mesothermal environments makes connellite a sought-after highlight in mineral cabinets, appreciated for both its aesthetic appeal and its insight into alteration processes in copper ore systems.